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Ground Water Information Depth and Gradient Live Oak reviewed ground-water elevation information available from the San Joaquin County Flood Control and Water Conservation District to determine the ground-water levels near the Site. Data from the fall of 2024 and spring of 2025 were the most recent available from this source. According to an analysis of these maps (Plates 5 through 8), depth to water in the area is approximately 12 to 13 feet, and ground water appears to flow generally to the northeast in the area at a rate of approximately 5 to 11 feet per mile. Live Oak excavated a ground-water boring to 11.50 feet below ground surface concurrent with the drilling of the percolation test hole. Ground water was encountered at 11.25 feet below ground surface. Potential Ground Water Contamination Issues The Soil Suitability Study is not intended to be an investigation into ground-water contamination sources, and no such investigation was conducted. Many sources can contribute to ground-water contamination, including leaking underground storage tanks, agricultural activities, dairies, septic systems, and storm water infiltration. Agricultural activities and the use of septic systems in the area are known ground-water contamination sources with the potential to impact the Site. Two common ground-water contaminants in San Joaquin County are nitrate and dibromochloropropane (DBCP). Live Oak reviewed the San Joaquin County Environmental Health Department's maps of Nitrate — Land Use Data and DBCP— Land Use Data dated October 2021. According to the nitrate map (Plate 9), five wells within a one-mile radius surrounding the subject Site have been tested. Nitrate was detected in two of the wells at concentrations between 0.1 and 5.0 mg/L-N and in two of the wells at concentrations between 5.1 and 10.0 mg/L-N; no nitrate was detected in the final well. Two wells within a one-mile radius surrounding the Site were tested for DBCP (Plate 10). DBCP was detected at a concentration between 0.01 and 0.2 µg/L in one well; no DBCP was detected in the other. Nitrate is commonly detected in shallow ground water aquifers of the Central Valley. Application of fertilizers, livestock waste, and untreated septic tank waste can all contribute to nitrate in ground water. Nitrate is mobile and tends to accumulate in shallow ground water zones. Based on work in the Sacramento Valley from the early 1900s, it is estimated that under "natural" conditions, ground water contains nitrate at concentrations no more than about 3 mg/L-N. Nitrate may be increasing in areas with LOGE 2606 Page 3